001445715 000__ 03845cam\a2200565Ii\4500
001445715 001__ 1445715
001445715 003__ OCoLC
001445715 005__ 20230310003846.0
001445715 006__ m\\\\\o\\d\\\\\\\\
001445715 007__ cr\un\nnnunnun
001445715 008__ 220407s2022\\\\sz\\\\\\ob\\\\001\0\eng\d
001445715 019__ $$a1309868640$$a1310333199
001445715 020__ $$a3030951936$$qelectronic book
001445715 020__ $$a9783030951931$$q(electronic bk.)
001445715 020__ $$z9783030951924
001445715 020__ $$z3030951928
001445715 0247_ $$a10.1007/978-3-030-95193-1$$2doi
001445715 035__ $$aSP(OCoLC)1309129665
001445715 040__ $$aYDX$$beng$$erda$$cYDX$$dYDX$$dN$T$$dOCLCO$$dGW5XE$$dEBLCP$$dOCLCO$$dOCLCF$$dOCLCQ
001445715 043__ $$an-us---
001445715 049__ $$aISEA
001445715 050_4 $$aS591$$b.L67 2022
001445715 08204 $$a631.4$$223/eng/20220408
001445715 1001_ $$aLorenz, Klaus$$q(Klaus Eugen),$$eauthor.
001445715 24510 $$aSoil organic carbon sequestration in terrestrial biomes of the United States /$$cKlaus Lorenz, Rattan Lal.
001445715 264_1 $$aCham :$$bPalgrave Macmillan,$$c2022.
001445715 300__ $$a1 online resource
001445715 336__ $$atext$$btxt$$2rdacontent
001445715 337__ $$acomputer$$bc$$2rdamedia
001445715 338__ $$aonline resource$$bcr$$2rdacarrier
001445715 504__ $$aIncludes bibliographical references and index.
001445715 5050_ $$a1. Introduction -- 1.1. Terrestrial Land Area -- 1.2. Principal Biomes of the U.S.A. -- 1.3. Changes in the Terrestrial Biosphere by Human Activities -- 2. Soil Organic Carbon Stocks -- 3. Soil Organic Carbon Sequestration -- 4. Soil Inorganic Carbon Stocks in Different Terrestrial Biomes -- 5. Conclusions -- 6. The Way Forward -- 7. Appendices.
001445715 506__ $$aAccess limited to authorized users.
001445715 520__ $$aTerrestrial biomes have soil organic carbon (SOC) stocks determined by natural (e.g., vegetation cover, soil type, climate) and anthropogenic (e.g., soil and land-use management) factors. Thus, biome type is among the main control of SOC stocks. Historically, many terrestrial biomes in the United States of America (U.S.A.) had higher SOC stocks than the same regions store today, and this discrepancy has contributed to increases in atmospheric carbon dioxide (CO2) concentrations and soil degradation. However, losses of SOC stocks must be reduced and/or stocks increased by SOC sequestration as net increases in SOC stocks contribute to climate change adaptation and mitigation by storing atmospheric CO2 in protected and stabilized fractions for millennia. Increases in SOC stocks will also contribute to improved soil fertility and soil health. Therefore, the aim of this book is to collate, review and synthesize information on how SOC stocks differ among major terrestrial biomes of the U.S.A. Information on soil inorganic carbon (SIC) stocks for different terrestrial biomes of the U.S.A. will also be presented. The book deliberates options for increasing SOC stocks and enhancing SOC sequestration in terrestrial biomes by soil and land-use management practices. It concludes with an overview of terrestrial biomes of the U.S.A. where targeted soil and land-use management practices may result in the greatest increases in SOC stocks and enhancements in SOC sequestration.
001445715 588__ $$aDescription based upon online resource; title from PDF title page (viewed April 8, 2022).
001445715 650_0 $$aSoils$$xCarbon content.
001445715 650_0 $$aCarbon sequestration$$zUnited States.
001445715 650_0 $$aSoil management$$zUnited States.
001445715 650_6 $$aSols$$xTeneur en carbone.
001445715 650_6 $$aPiégeage du carbone$$zÉtats-Unis.
001445715 650_6 $$aSols$$xAménagement$$zÉtats-Unis.
001445715 655_0 $$aElectronic books.
001445715 7001_ $$aLal, R.,$$eauthor.
001445715 77608 $$iPrint version:$$z3030951928$$z9783030951924$$w(OCoLC)1289478975
001445715 852__ $$bebk
001445715 85640 $$3Springer Nature$$uhttps://univsouthin.idm.oclc.org/login?url=https://link.springer.com/10.1007/978-3-030-95193-1$$zOnline Access$$91397441.1
001445715 909CO $$ooai:library.usi.edu:1445715$$pGLOBAL_SET
001445715 980__ $$aBIB
001445715 980__ $$aEBOOK
001445715 982__ $$aEbook
001445715 983__ $$aOnline
001445715 994__ $$a92$$bISE